Books on the topic 'Freshwater biota'

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1

Pleshanov, A. S., A. N. Matveev, and N. M. Pronin. Biota Vitimskogo zapovednika: Struktura bioty vodnykh ėkosistem. Novosibirsk: Geo, 2006.

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2

Bird, G. A. Nuclide concentration factors for freshwater biota. Pinawa, Man: AECL, Whiteshell Laboratories, 1996.

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3

Setyadi, Gesang. Biota akuatik di perairan Mimika, Papua. Jakarta]: Freeport Indonesia, 2002.

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4

Adolphson, Debbie L. Habitat, biota, and sediment characteristics at selected stations in the lower Illinois River Basin, Illinois, 1996-98. Urbana, Ill: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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5

Adolphson, Debbie L. Habitat, biota, and sediment characteristics at selected stations in the lower Illinois River Basin, Illinois, 1996-98. Urbana, Ill: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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6

Adolphson, Debbie L. Habitat, biota, and sediment characteristics at selected stations in the lower Illinois River Basin, Illinois, 1996-98. Urbana, Ill: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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7

Paul, Marsh, ed. Inland fishes of the greater Southwest: Chronicle of a vanishing biota. Tucson: University of Arizona Press, 2009.

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8

Adolphson, Debbie L. Habitat, biota, and sediment characteristics at selected stations in the lower Illinois River Basin, Illinois, 1996-98. Urbana, Ill: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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9

Oceans, Canada Department of Fisheries and. Acidification of surface waters in eastern Canada and its relationship to aquatic biota. Ottawa: Department of Fisheries and Oceans, 1987.

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10

Grasso, Dennis N. Field screening of water quality, bottom sediment, and biota associated with irrigation drainage, Wind River Indian Reservation, Wyoming, 1992-93. Cheyenne, Wyo: U.S. Dept. of the Interior, U.S. Geological Survey, 1995.

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11

Braun, Christopher L. Baseline assessment of physical characteristics, aquatic biota, and selected water-quality properties at the reach and mesohabitat scale for reaches of Big Cypress, Black Cypress, and Little Cypress bayous, Big Cypress Basin, northeastern Texas, 2010-2011. Reston, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2013.

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12

D, Capel Paul, and Dileanis Peter D, eds. Pesticides in stream sediment and aquatic biota: Distribution, trends, and governing factors. Boca Raton, Fla: Lewis Publishers, 1999.

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13

Embrey, S. S. Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the Columbia Basin Project, Washington, 1991-92. Tacoma, Wash: U.S. Dept. of the Interior, U.S. Geological Survey, 1995.

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14

International, Conference on Fluvial Sedimentology (6th 1997 Cape Town South Africa). Catchment influences on the geomorphology and biota of the Sabie and Letaba Rivers in the Kruger National Park: Pre-conference field excursion, 6th International Conference on Fluvial Sedimentology, University of Cape Town, South Africa, 15 to 20 September, 1997. [Cape Town, South Africa: The Conference, 1997.

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15

Rinella, Frank A. Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the Owyhee and Vale Projects, Oregon and Idaho, 1990-91. Portland, Or: U.S. Dept. of the Interior, U.S. Geological Survey, 1994.

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16

(Editor), Peter Calow, and Geoffrey E. Petts (Editor), eds. River Biota: Selected Extracts from the Rivers Handbook. Blackwell Publishing Limited, 1996.

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17

Dalu, Tatenda, and Ryan J. Wasserman. Tropical Freshwater Wetlands: From Abiotic and Biota to Conservation Management. Elsevier, 2021.

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18

Marsh, Paul C., and W. L. Minckley. Inland Fishes of the Greater Southwest: Chronicle of a Vanishing Biota. University of Arizona Press, 2016.

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19

New Jersey. Toxics in Biota Committee., ed. Mercury contamination in New Jersey freshwater fish: Report of the Toxics in Biota Committee. [Trenton, N.J.]: New Jersey Dept. of Environmental Protection, 1994.

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20

Rogers, Kerrylee, and Timothy J. Ralph, eds. Floodplain Wetland Biota in the Murray-Darling Basin. CSIRO Publishing, 2010. http://dx.doi.org/10.1071/9780643100992.

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Floodplain wetlands of the Murray-Darling Basin provide critical habitat for numerous species of flora and fauna, yet the ecology of these wetlands is threatened by a range of environmental issues. This book addresses the urgent need for an improved ecohydrological understanding of the biota of Australian freshwater wetlands. It synthesises key water and habitat requirements for 35 species of plants, 48 species of waterbirds, 17 native and four introduced species of fish, 15 species of frogs, and 16 species of crustaceans and molluscs found in floodplain wetlands of the Murray-Darling Basin. Each species profile includes: the influence of water regimes on the survival, health and condition of the species; key stimuli for reproduction and germination; habitat and dietary preferences; as well as major knowledge gaps for the species. Floodplain Wetland Biota in the Murray-Darling Basin also provides an overview of the likely impacts of hydrological change on wetland ecosystems and biota, in the context of climate change and variability, with implications for environmental management. This important book provides an essential baseline for further education, scientific research and management of floodplain wetland biota in the Murray-Darling Basin.
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21

Nowell, Lisa H. Pesticides in Stream Sediment and Aquatic Biota: Distribution, Trends, and Governing Factors. Taylor & Francis Group, 2019.

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22

Nowell, Lisa H. Pesticides in Stream Sediment and Aquatic Biota: Distribution, Trends, and Governing Factors. Taylor & Francis Group, 2019.

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23

Nowell, Lisa H. Pesticides in Stream Sediment and Aquatic Biota: Distribution, Trends, and Governing Factors. Taylor & Francis Group, 2019.

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24

Nowell, Lisa H. Pesticides in Stream Sediment and Aquatic Biota: Distribution, Trends, and Governing Factors. Taylor & Francis Group, 2019.

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25

Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in and near Humboldt Wildlife Management Area, Churchill and Pershing counties, Nevada, 1990-91. Carson City, Nev: U.S. Geological Survey, 1993.

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26

Capel, Paul D., Lisa H. Nowell, and Peter D. Dileanis. Pesticides in Stream Sediment and Aquatic Biota: Distribution, Trends, and Governing Factors (Pesticides in the Hydrologic System, V. 4). CRC, 1999.

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27

Vuorinen, Ilppo. Post-Glacial Baltic Sea Ecosystems. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.675.

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Post-glacial aquatic ecosystems in Eurasia and North America, such as the Baltic Sea, evolved in the freshwater, brackish, and marine environments that fringed the melting glaciers. Warming of the climate initiated sea level and land rise and subsequent changes in aquatic ecosystems. Seminal ideas on ancient developing ecosystems were based on findings in Swedish large lakes of species that had arrived there from adjacent glacial freshwater or marine environments and established populations which have survived up to the present day. An ecosystem of the first freshwater stage, the Baltic Ice Lake initially consisted of ice-associated biota. Subsequent aquatic environments, the Yoldia Sea, the Ancylus Lake, the Litorina Sea, and the Mya Sea, are all named after mollusc trace fossils. These often convey information on the geologic period in question and indicate some physical and chemical characteristics of their environment. The ecosystems of various Baltic Sea stages are regulated primarily by temperature and freshwater runoff (which affects directly and indirectly both salinity and nutrient concentrations). Key ecological environmental factors, such as temperature, salinity, and nutrient levels, not only change seasonally but are also subject to long-term changes (due to astronomical factors) and shorter disturbances, for example, a warm period that essentially formed the Yoldia Sea, and more recently the “Little Ice Age” (which terminated the Viking settlement in Iceland).There is no direct way to study the post-Holocene Baltic Sea stages, but findings in geological samples of ecological keystone species (which may form a physical environment for other species to dwell in and/or largely determine the function of an ecosystem) can indicate ancient large-scale ecosystem features and changes. Such changes have included, for example, development of an initially turbid glacial meltwater to clearer water with increasing primary production (enhanced also by warmer temperatures), eventually leading to self-shading and other consequences of anthropogenic eutrophication (nutrient-rich conditions). Furthermore, the development in the last century from oligotrophic (nutrient-poor) to eutrophic conditions also included shifts between the grazing chain (which include large predators, e.g., piscivorous fish, mammals, and birds at the top of the food chain) and the microbial loop (filtering top predators such as jellyfish). Another large-scale change has been a succession from low (freshwater glacier lake) biodiversity to increased (brackish and marine) biodiversity. The present-day Baltic Sea ecosystem is a direct descendant of the more marine Litorina Sea, which marks the beginning of the transition from a primeval ecosystem to one regulated by humans. The recent Baltic Sea is characterized by high concentrations of pollutants and nutrients, a shift from perennial to annual macrophytes (and more rapid nutrient cycling), and an increasing rate of invasion by non-native species. Thus, an increasing pace of anthropogenic ecological change has been a prominent trend in the Baltic Sea ecosystem since the Ancylus Lake.Future development is in the first place dependent on regional factors, such as salinity, which is regulated by sea and land level changes and the climate, and runoff, which controls both salinity and the leaching of nutrients to the sea. However, uncertainties abound, for example the future development of the Gulf Stream and its associated westerly winds, which support the sub-boreal ecosystems, both terrestrial and aquatic, in the Baltic Sea area. Thus, extensive sophisticated, cross-disciplinary modeling is needed to foresee whether the Baltic Sea will develop toward a freshwater or marine ecosystem, set in a sub-boreal, boreal, or arctic climate.
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